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SCHRIFTENREIHE Institut für Pflanzenernährung und Bodenkunde ...

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Chapter 1 Introduction<br />

is also uncertain. Thus, the hydraulic model, linked with representative of<br />

monitoring locations, should be more valuable to get a comparable conclusion<br />

considering spatial variability.<br />

year<br />

month<br />

day<br />

hour<br />

aggregate<br />

soil moisture<br />

regime<br />

grazing effect<br />

aggregation<br />

1D- modeling<br />

soil moisture<br />

water flux<br />

scaling<br />

flow<br />

separation<br />

HYDRUS<br />

model<br />

2D- modeling<br />

water budget<br />

computing<br />

hydrograph<br />

rainfall etc.<br />

plot catena catchment<br />

Fig. 1.2. Methodology to <strong>und</strong>erstand and quantify the hydrological processes at different<br />

spatio-temporal scales (personal communications with Prof H. Zepp, Ruhr-University<br />

Bochum, Germany; 2004).<br />

Land management is reported to influence soil hydraulic and thermal properties<br />

by altering soil and plant functions (Flerchinger et al., 2003). In pasture areas,<br />

soil mechanical disturbances due to animal trampling, interlinked with<br />

hydrological changes, often have detrimental effects on soil properties.<br />

Particularly in the topsoil, soil deformation is characterized by a decrease of pore<br />

volume and an altered pore size distribution, which both affect water and air<br />

conductivity (Willat and Pullar, 1983; Krümmelbein et al., 2006), and soil water<br />

retention characteristics (Martinez and Zinck, 2004; Kutilek et al., 2006). These<br />

disturbances of soil structure further decrease water infiltrability and increase<br />

surface runoff. This will not only cause soil erosion by water and nutrient<br />

3

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